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Establishing 3D hydrogeological solid model and database for sustainable groundwater management in the Vietnam Mekong delta
Author(s) -
Vu Thanh Tam,
AUTHOR_ID,
Nguyễn Ngọc Hà,
Ho Van Thuy,
AUTHOR_ID,
AUTHOR_ID
Publication year - 2021
Publication title -
vietnam journal of science, technology and engineering (ministry of science and technology)/vietnam journal of science, technology and engineering
Language(s) - English
Resource type - Journals
eISSN - 2615-9937
pISSN - 2525-2461
DOI - 10.31276/vjste.63(4).86-94
Subject(s) - hydrogeology , groundwater , aquifer , delta , geology , saltwater intrusion , subsidence , structural basin , quaternary , hydrology (agriculture) , water resource management , environmental science , geomorphology , paleontology , geotechnical engineering , aerospace engineering , engineering
The Vietnam Mekong delta (VMD) is a tide-dominated delta formed by the Mekong river system. The sediments are dominantly fine grained and were deposited in the receiving basin with slight inclination of pre-existing deposits in the East sea and gulf of Thailand. The VMD is homeland to about 18 million people that exploit about 4-6 million m3/day of groundwater mainly for domestic use. In recent years, significant groundwater depletion has been occurring in many parts of the VMD due to excessive pumping. Consequently, the VMD has become increasingly faced with serious land subsidence, salt groundwater intrusion, and contamination. Establishing a 3D hydrogeological solid model and database are sorely needed to achieve sustainable groundwater management, and to serve as a basis for further in-depth analyses to quantify contributions from the above-mentioned hazards to current hydrogeological conditions. Therefore, a 3D hydrogeological solid model and database were built based on more than 1000 well logs available from the VMD. An areal distribution of the Holocene, Pleistocene, Pliocene, and Late Miocene subsurfaces from this 3D hydrogeological solid model and database showed zones of tectonic depression and uplift from Early Miocene - Quaternary. Also, the resulting areal distribution aquitards and aquifers thicknesses gave hints of ground saltwater intrusion and contamination.

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